Seasonal and Spatial Distribution of Phosphates, Nitrates, and Silicates in Lake Champlain, U.S.A.

Abstract

A study of the limnological characteristics was conducted from January through November, 1970 of Lake Champlain, Vermont and New York, U.S.A. The seasonal and spatial distribution of soluble nitrate, total phosphate and reactive silicate concentrations from 20 stations are presented here.

Results for soluble nitrate concentrations indicate that concentrations in the northeast area of the lake are significantly lower throughout the year than the open lake and bay stations in the western main portion of the lake. Three of the shallow bay stations generally had higher concentrations of nitrate than all other stations. Concentrations of reactive silicon dioxide do not show the same general trends as the nitrata data. Silicate concentrations in the western open portions are higher in the winter and lower in the summer than other areas. The northeast arm does not show the dramatic difference in silicates as for nitrate concentrations. The shallow bays had significantly higher silicate concentrations also, especially during peak spring runoff. No detectable soluble phosphate was measured in the surface waters of the lake. Total particulate phosphate concentrations remained relatively constant from station to station, and throughout the season.

The results of the measurements of soluble nitrate and silicate generally support the hypothesis that Lake Champlain is composed of a number of distinct water masses. The general pattern of total phosphate concentrations however, does not support this hypothesis. A comparison of the three major nutrients in Lake Champlain with the St. Lawrence Great Lake indicates that the trophic status of Lake Champlain is generally higher than Lake Superior and very similar to the open waters of Lake Michigan and Lake Huron.